Kryostega collinsoni

Kryostega is a large temnospondyl amphibian from the Early or Middle Triassic of Antarctica. The genus is based on a single specimen collected in 1986 by a team led by paleontologist William H. Hammer of Augustana College, and now housed in the collections of the American Museum of Natural History.

Kryostega collinsoni

Jonathan Chen · CC BY-SA 4.0 · via Wikipedia/Commons. May be a photograph of a specimen, or an artist’s reconstruction — an interpretation of a skeleton, since colour and soft tissue are almost never preserved.

On record

Recorded, not inferred
Sits inside
KryostegaPBDB
Diet
carnivorePBDB, for Temnospondyli
Life habit
amphibiousPBDB, for Temnospondyli
Motility
actively mobilePBDB, for Temnospondyli
Environment
brackish,freshwater,terrestrialPBDB, for Tetrapoda

Time the record covers

At most 5.6 million years on record.

The one occurrence read is dated to somewhere between 247 Mya and 241.464 Mya, which is a dating window rather than a span.

Early Triassic — about 0 of 1 occurrenceMiddle Triassic — about 1 of 1 occurrenceMiddle Triassic247–247 Mya — about 0.0 occurrences247–247 Mya — about 0.0 occurrences247–246 Mya — about 0.0 occurrences246–246 Mya — about 0.0 occurrences246–246 Mya — about 0.0 occurrences246–246 Mya — about 0.0 occurrences246–246 Mya — about 0.0 occurrences246–245 Mya — about 0.0 occurrences245–245 Mya — about 0.0 occurrences245–245 Mya — about 0.0 occurrences245–245 Mya — about 0.0 occurrences245–244 Mya — about 0.0 occurrences244–244 Mya — about 0.0 occurrences244–244 Mya — about 0.0 occurrences244–244 Mya — about 0.0 occurrences244–244 Mya — about 0.0 occurrences244–243 Mya — about 0.0 occurrences243–243 Mya — about 0.0 occurrences243–243 Mya — about 0.0 occurrences243–243 Mya — about 0.0 occurrences243–242 Mya — about 0.0 occurrences242–242 Mya — about 0.0 occurrences242–242 Mya — about 0.0 occurrences242–242 Mya — about 0.0 occurrences242–242 Mya — about 0.0 occurrences242–241 Mya — about 0.0 occurrences247.5 Mya241 Mya

1 occurrence of Kryostega collinsoni on record, most of them in the Middle Triassic. Bar height is expected occurrences, not a count: each fossil is spread across the span it is dated to, so a tall narrow bar means tight dating and a low wide one means loose.

When

1 occurrences

These are dates about fossils, not the animal: the record can only begin after it arose and end before it died out, so either end may reach further. Shares are expected occurrences: a fossil dated to a span is counted partly in each period it straddles. More on what this infers.

Found in

1 formation

Fremouw — 84.35°S, 164.05°E

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The named rock units Kryostega collinsoni has been recovered from, largest first. Drawn where the rock is now, not where it formed.

Kryostega collinsoni and its relatives

Middle Triassic

Where Kryostega collinsoni and its relatives were recorded in the Middle Triassic.

Found in the same rock

6 taxa

The Paleobiology Database records 1 site for Kryostega collinsoni, and this reads all of them. The number is how many of those sites it was catalogued from too.

This is not a list of everything alive at the time. It is only what has come out of the same ground as this animal and been written down.

Entered from

1 reference

Each of the 1 occurrence read was entered from one of these publications, ordered by how many each accounts for. This is not a search for papers mentioning the name. Each entry links to doi.org. Relayed as the Paleobiology Database holds them, not checked against what they resolve to.

Media and terms

Media content1

Picture of Kryostega collinsoni

Credit
Jonathan Chen
Licence
CC BY-SA 4.0
Commercial use
the licence allows it

No 3D scan of Kryostega collinsoni was found in Sketchfab.

Smithsonian Open Access and MorphoSource were not reached for this taxon, so this list is what the others held rather than everything there is.

The description on this site

Licence
CC BY-SA 4.0

This is what the site found, which is not the same as what exists.

Keep going

Occurrence data from the Paleobiology Database, CC BY 4.0. Sidor et al. 2008